Search results for "Flow"

showing 10 items of 5185 documents

Climate signatures on decadal to interdecadal time scales as obtained from mollusk shells (Arctica islandica) from Iceland

2013

Abstract Pronounced decadal climate oscillations are detected in a multi-centennial record based on shell growth rates of the marine bivalve mollusk, Arctica islandica, from Iceland. The corresponding analysis of patterns in sea level pressure and temperature exhibit large-scale teleconnections with North Atlantic climate quantities. We find that the record projects onto blocking situations in the northern North Atlantic. The associated circulation shows a low-pressure signature over Greenland and the Labrador Sea and a high-pressure system over Western Europe associated with northeasterly flow towards Iceland and weakening in the westerly zonal flow over Europe. It can be speculated that s…

geographyAlkenonegeography.geographical_feature_category010504 meteorology & atmospheric sciencesbiologyBivalve molluskAtmospheric circulationPaleontology010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesOceanography13. Climate actionClimatologyZonal flowAtlantic multidecadal oscillationSea ice14. Life underwaterArctica islandicaEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTeleconnectionPalaeogeography, Palaeoclimatology, Palaeoecology
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Shallow urban aquifers under hyper-recharge equatorial conditions and strong anthropogenic constrains. Implications in terms of groundwater resources…

2021

Abstract Humid equatorial regions are recognized as the least documented in term of hydrogeological functioning of aquifers despite the fact that they house a lot of developing countries and that groundwater is often the main water resource. Regarding this aspect, a study was conducted in sub-Saharan Africa, focusing on the Mio-Pliocene aquifer in Douala megacity (Cameroon) which is the rainiest city in West-Africa (about 4000 mm/year) with one of the greatest demographic growth rate of the African continent. Firstly, groundwater recharge rate has been calculated through water balance and Water Table Fluctuation methods. Results show that the aquifer is characterized by a high recharge of 6…

geographyEnvironmental Engineeringgeography.geographical_feature_category010504 meteorology & atmospheric sciencesGroundwater flowWater tableAquiferGroundwater recharge010501 environmental sciences01 natural sciencesPollution6. Clean waterRainwater harvestingWater balance13. Climate action[SDE]Environmental SciencesVadose zoneEnvironmental ChemistryEnvironmental scienceWater resource managementWaste Management and DisposalComputingMilieux_MISCELLANEOUSGroundwater0105 earth and related environmental sciencesScience of The Total Environment
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Management of irrigation water and nutrient demands of tomato (Lycopersicon esculentum Mill.) using urban treated wastewater from a pilot-scale horiz…

2017

The reuse of treated wastewater (TWW) in crop irrigation is an advanced and rational approach to water resource management in agriculture. Results would seem to demonstrate that it could be an extremely important tool in the reduction of freshwater (FW) consumption in agriculture, at the same time helping to increase crop yields through the transfer of nutrients required for crop growth. In arid and semi-arid areas of the Mediterranean, constructed wetlands can play a key role in the treatment and reuse of wastewater due to their multifunctional nature. The aim of this study was to manage water and nutrient requirements of tomato (Lycopersicon esculentum Mill.) using TWW from a pilot-scale …

geographyIrrigationgeography.geographical_feature_categoryEnvironmental engineeringWetlandN P K supply02 engineering and technology010501 environmental sciences01 natural sciencesPhytoremediationSettore AGR/02 - Agronomia E Coltivazioni ErbaceeWater resources020401 chemical engineeringWastewaterSoil pHConstructed wetlandFreshwater savingEnvironmental scienceIrrigation and fertilizationSewage treatmentAgricultural crop0204 chemical engineeringSubsurface flow0105 earth and related environmental sciences
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Assessing dye-tracer technique for rill flow velocity measurements

2018

Abstract Rill erosion is considered one of the most important processes affecting soil because of the large amount of soil loss. The rill network acts as sediment source and is able to transport both rill flow-detached particles and those delivered from the interrill areas. Small flow depth in a rill and steep slope values of its bed affect significantly flow hydraulics. When rill flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measured surface velocity of the leading edge of the tracer plume by a correction factor. The main uncertainty of the dye-tracing technique stands in the relationship between mean and surface flow velocity. In …

geographyLeading edgegeography.geographical_feature_categoryCorrection factorDye methodHydraulics0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyDarcy–Weisbach equation020801 environmental engineeringPlumelaw.inventionRillFlow velocityFlow resistanceFlow velocitylawTRACERRill flowSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeologyEarth-Surface Processes
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Exceptional mobility of an advancing rhyolitic obsidian flow at Cordón Caulle volcano in Chile

2013

The emplacement mechanisms of rhyolitic lava flows are enigmatic and, despite high lava viscosities and low inferred effusion rates, can result in remarkably, laterally extensive (30 km) flow fields. Here we present the first observations of an active, extensive rhyolitic lava flow field from the 2011-2012 eruption at Cordón Caulle, Chile. We combine high-resolution four-dimensional flow front models, created using automated photo reconstruction techniques, with sequential satellite imagery. Late-stage evolution greatly extended the compound lava flow field, with localized extrusion from stalled, ~35 m-thick flow margins creating80 breakout lobes. In January 2013, flow front advance continu…

geographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesLavaGeneral Physics and AstronomySilicicGeneral Chemistry010502 geochemistry & geophysics01 natural sciencesFlow fieldGeneral Biochemistry Genetics and Molecular BiologyFlow (mathematics)VolcanoRhyolitePetrologyGeology0105 earth and related environmental sciencesNature Communications
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Modelling of piping collapses and gully headcut landforms: Evaluating topographic variables from different types of DEM

2021

Abstract The geomorphic studies are extremely dependent on the quality and spatial resolution of digital elevation model (DEM) data. The unique terrain characteristics of a particular landscape are derived from DEM, which are responsible for initiation and development of ephemeral gullies. As the topographic features of an area significantly influences on the erosive power of the water flow, it is an important task the extraction of terrain features from DEM to properly research gully erosion. Alongside, topography is highly correlated with other geo-environmental factors i.e. geology, climate, soil types, vegetation density and floristic composition, runoff generation, which ultimately inf…

geographyQE1-996.5geography.geographical_feature_category010504 meteorology & atmospheric sciencesAdvanced land observation satellite (ALOS)Water flowLandformCforestGully erosion susceptibility (GES)ElevationElastic netTerrainCubistGeologyVegetation010502 geochemistry & geophysics01 natural sciencesAdvanced Spaceborne Thermal Emission and Reflection RadiometerGeneral Earth and Planetary SciencesSurface runoffDigital elevation modelGeomorphologyDigital elevation model (DEM)Geology0105 earth and related environmental sciencesGeoscience Frontiers
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The percolation threshold and permeability evolution of ascending magmas

2017

Abstract The development of gas permeability in magmas is a complex phenomenon that directly influences the style of a volcanic eruption. The emergence of permeability is linked to the concept of percolation threshold, which is the point beyond which gas bubbles are connected in a continuous network that allows gas escape. Measurements of the percolation threshold, however, range from ∼30 to 78 vol%. No known combination of parameters can explain such a wide range of threshold values, which affects our understanding of the relationship between percolation and permeability. We present permeability calculations on bubble-bearing rhyolitic melts that underwent experimental decompression. Sampl…

geographyVulcanian eruptiongeography.geographical_feature_category010504 meteorology & atmospheric sciencesBubbleMineralogyPercolation thresholdMechanicsPermeability coefficient010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsPermeability (earth sciences)GeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Conduit flowOrder of magnitudeGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Comment on “Effects of different tillage practices on the hydraulic resistance of concentrated flow on the loess plateau in China” by J. Sun et al

2020

Abstract For concentrated flows, which are characterized by small water depth and steep sloping beds, hydraulic conditions different from those typical of streams and rivers occur. In this study a new theoretically deduced flow resistance equation was tested using the experimental data by Sun et al. for three different tilled surfaces (Manual Dibbling, MD, Manual Hoeing, MH, and Contour Drilling, CD). At first, the profile parameter-relationship, which is the relationship between the velocity profile parameter Γ, the channel slope and the flow Froude number, was calibrated using rill flow data by Di Stefano et al. Then, the applicability of this relationship was tested by the measurements o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFlow (psychology)Soil science04 agricultural and veterinary sciencesSurface finish01 natural sciencesTillageRillsymbols.namesakeFlow velocity040103 agronomy & agricultureFroude numbersymbolsCalibrationSurface roughness0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDimensional analysis Flow resistance Self-similarity Soil erosion Velocity profileGeology0105 earth and related environmental sciencesEarth-Surface Processes
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2016

Recent gas flux measurements have shown that Strombolian explosions are often followed by periods of elevated flux, or “gas codas,” with durations of order a minute. Here we present UV camera data from 200 events recorded at Stromboli volcano to constrain the nature of these codas for the first time, providing estimates for combined explosion plus coda SO2 masses of ≈18–225 kg. Numerical simulations of gas slug ascent show that substantial proportions of the initial gas mass can be distributed into a train of “daughter bubbles” released from the base of the slug, which we suggest, generate the codas, on bursting at the surface. This process could also cause transitioning of slugs into cap b…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesbusiness.industryFlow (psychology)FluxGeophysicsComputational fluid dynamicsVolcanic explosivity index010502 geochemistry & geophysics01 natural sciencesStrombolian eruptionGeophysicsElectrical conduitVolcano13. Climate actionGas slugGeneral Earth and Planetary SciencesbusinessGeology0105 earth and related environmental sciencesGeophysical Research Letters
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Water resource assessment in karst and fractured aquifers of Termini Imerese-Trabia Mts. (Northern central Sicily, Italy).

2014

The carbonatic siliciclastic Mesozoic reliefs of Termini Imerese-Trabia Mts. (Northern central Sicily) were selected in order to investigate groundwater resources, as these fissured to karstic aquifers are used for potable water supply. These reliefs, part of the Sicilian Apennine Chain, consist of a tectonic units (deformed and emplaced during the Miocene-Pleistocene, and collapsed during the Plio-Pleistocene) mostly formed by clayey pelagic limestones (Sicilidi domain) overthrusting Meso-Cenozoic carbonate and silicoclastic rocks (Imerese Basin, Late Triassic-Early Oligocene) and terrigenous covers (Numidian Flysch, Late Oligocene-Early Miocene). The evolution of karstic network and subsu…

geographygeography.geographical_feature_categoryFlyschGroundwater flowTerrigenous sedimentSettore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistryAquiferStructural basinKarstSiliciclasticGeomorphologyGroundwaterGeologyAquifers karst
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